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The article discusses the research study conducted to examine the geodynamic setting and tectonic model of porphyry copper?gold deposits in West Junggar, northwest China in the Central Asia Orogenic Belt (CAOB). It mentions that the porphyry deposit is associated with a late carboniferous intrusive complex. It reveals that the ore-bearing porphyry system was derived from partial melting of multiple sources including oceanic crust and a subduction-modified mantle wedge in paleo-Junggar ocean.